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Stuartia (protista) ( шпански; кастиљски )

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Stuartia es un género de foraminífero bentónico de la familia Fursenkoinidae, de la superfamilia Fursenkoinoidea, del suborden Buliminina y del orden Buliminida.[1][2]​ Su especie tipo es Stuartia ruthae. Su rango cronoestratigráfico abarca el Holoceno.

Discusión

Clasificaciones previas incluían Stuartia en el suborden Rotaliina del orden Rotaliida.[3]

Clasificación

Stuartia incluye a las siguientes especies:[4][5]

Bibliografía

  1. Loeblich, A.R., Jr. y Tappan, H. (1992). Present Status of Foraminiferal Classification. Studies in Benthic Foraminifera en Benthos'90, Sendai (1990), Tokai University Press, 93-102.
  2. World Modern Foraminifera Database, en http://www.marinespecies.org/foraminifera/index.php
  3. Loeblich, A.R., Jr. y Tappan, H. (1987). Foraminiferal genera and their classification. Van Nostrand Reinhold Company (ed.), 2 vol., 1-970, 1-212 + 847 láminas.
  4. Encyclopedia of the Life, en http://eol.org/
  5. Classifications Browser en http://www.ubio.org/browser/classifications.php?conceptID=13894357&expand=1&namebankID= Página 1 de 134
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Stuartia (protista): Brief Summary ( шпански; кастиљски )

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Stuartia es un género de foraminífero bentónico de la familia Fursenkoinidae, de la superfamilia Fursenkoinoidea, del suborden Buliminina y del orden Buliminida.​​ Su especie tipo es Stuartia ruthae. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis ( англиски )

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Test elongate, flattened, palmate in outline, biserial, chambers broad and low and sutures strongly oblique on the dorsal side, chambers more strongly overlapping and sutures less oblique on the ventral side where the final pair of chambers comprises about one-half the test, proximal margin of chambers truncated, with a sharp and commonly fimbriate border and with lateral spinelike projections resulting in a serrate margin, sutures depressed; wall calcareous, finely perforate, glossy, surface smooth except for the fimbriate or serrate lower chamber margin; aperture an elongate slit paralleling the margin on the ventral side, extending from the base of the chamber nearly to the test apex. Holocene; Pacific: off Bikini Island, at about 1,700 m to 2,300 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification)

Навод

Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp.

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Tomas Cedhagen [email]
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